Open AccessDescent toward the Icehouse: Eocene sea surface cooling inferred from GDGT distributions
Author(s) -
Inglis Gordon N.,
Farnsworth Alexander,
Lunt Daniel,
Foster Gavin L.,
Hollis Christopher J.,
Pagani Mark,
Jardine Phillip E.,
Pearson Paul N.,
Markwick Paul,
Galsworthy Amanda M. J.,
Raynham Lauren,
Taylor Kyle. W. R.,
Pancost Richard D.
Publication year - 2015
Publication title -
paleoceanography
Language(s) - English
Resource type - Journals
eISSN - 1944-9186
pISSN - 0883-8305
DOI - 10.1002/2014pa002723
Subject(s) - thaumarchaeota , geology , oceanography , sea surface temperature , paleontology , climatology , archaea , bacteria
The TEX 86 proxy, based on the distribution of marine isoprenoidal glycerol dialkyl glycerol tetraether lipids (GDGTs), is increasingly used to reconstruct sea surface temperature (SST) during the Eocene epoch (56.0–33.9 Ma). Here we compile published TEX 86 records, critically reevaluate them in light of new understandings in TEX 86 palaeothermometry, and supplement them with new data in order to evaluate long‐term temperature trends in the Eocene. We investigate the effect of archaea other than marine Thaumarchaeota upon TEX 86 values using the branched‐to‐isoprenoid tetraether index (BIT), the abundance of GDGT‐0 relative to crenarchaeol (%GDGT‐0), and the Methane Index (MI). We also introduce a new ratio, %GDGT RS , which may help identify Red Sea‐type GDGT distributions in the geological record. Using the offset between TEX 86 H and TEX 86 L (ΔH‐L) and the ratio between GDGT‐2 and GDGT‐3 ([2]/[3]), we evaluate different TEX 86 calibrations and present the first integrated SST compilation for the Eocene (55 to 34 Ma). Although the available data are still sparse some geographic trends can now be resolved. In the high latitudes (>55°), there was substantial cooling during the Eocene (~6°C). Our compiled record also indicates tropical cooling of ~2.5°C during the same interval. Using an ensemble of climate model simulations that span the Eocene, our results indicate that only a small percentage (~10%) of the reconstructed temperature change can be ascribed to ocean gateway reorganization or paleogeographic change. Collectively, this indicates that atmospheric carbon dioxide ( p CO 2 ) was the likely driver of surface water cooling during the descent toward the icehouse.